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Добірка наукової літератури з теми "North Shore of the St"

Автор: Grafiati
Опубліковано: 7 вересня 2024

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Статті в журналах з теми "North Shore of the St"

1

Ouellet, Jean-François, Pierre Fradette, and Isabel Blouin. "Do Barrow's Goldeneyes, Bucephala islandica, Breed South of the St. Lawrence Estuary in the Gaspé Peninsula, Eastern Canada?" Canadian Field-Naturalist 124, no. 2 (April 1, 2010): 179. http://dx.doi.org/10.22621/cfn.v124i2.1057.

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We report the first observations of Barrow's Goldeneyes south of the St. Lawrence estuary in typical breeding habitat during the breeding season. Until recently, the confirmed breeding locations for the species in Eastern North America were all located on the north shore of the Estuary and Gulf of St. Lawrence.
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2

Rail, Jean-François, and Gilles Chapdelaine. "Food of Double-crested Cormorants,Phalacrocorax auritus, in the Gulf and Estuary of the St. Lawrence River, Quebec, Canada." Canadian Journal of Zoology 76, no. 4 (April 1, 1998): 635–43. http://dx.doi.org/10.1139/z97-237.

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Between 1994 and 1996, a total of 613 Double-crested Cormorant (Phalacrocorax auritus) regurgitations were collected at four colonies located in the St. Lawrence Estuary and one colony on the North Shore of the Gulf of St. Lawrence. The diet comprised a great variety of prey, with fishes well represented. Capelin (Mallotus villosus) and sand lance (Ammodytes sp.) together constituted most of the diet, (i.e., frequency of occurrence 66%, numerical frequency 68%, and volume 50%). Sand lance, which were nearly absent in regurgitations from the Estuary, were important in the diet of cormorants from the North Shore of the Gulf. At the North Shore colony, capelin were much more abundant in the diet in 1996 than in 1995, which correlates with independent fisheries data. In contrast to the results of previous studies of this cormorant's diet, our results show a preponderance of schooling fishes over benthic species. We suggest that this reflects a recent trend towards an increase in the abundance of schooling fishes in the St. Lawrence Estuary and Gulf. Overfishing of predatory fishes and oceanographic factors could be involved.
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3

Mingelbier, M., F. Lecomte, and J. J. Dodson. "Climate change and abundance cycles of two sympatric populations of smelt (Osmerus mordax) in the middle estuary of the St. Lawrence River, Canada." Canadian Journal of Fisheries and Aquatic Sciences 58, no. 10 (October 1, 2001): 2048–58. http://dx.doi.org/10.1139/f01-140.

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Commercial catches of two ecologically distinct sympatric smelt (Osmerus mordax) populations segregated along the two shores of the St. Lawrence middle estuary exhibited inverse patterns with periodicities on the order of 30 years. The influence of water level in the St. Lawrence River and air temperature, chosen to reflect variations in hydrology and climate, differed markedly between the two populations. Analyses revealed that both water level and temperature were generally positively related with north-shore smelt landings and negatively related with south-shore smelt landings. For both populations, a number of significant climatic factors contributing to variance in smelt landings were lagged by one to three years relative to the year of landings, indicating that climatic variables influenced smelt recruitment. The contrasting role of hydroclimatic variables in driving these abundance cycles is likely related to differential exploitation of estuarine habitats; the south-shore population is associated with shallow shoal habitat, whereas the north-shore population is associated with deep channel habitat. The responses of the two smelt populations also reflect the fundamental ecological differences existing between shoal and channel habitats, indicating that future climate change may differentially affect other populations or species that are segregated between these two habitats.
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4

Assani, Ali Arkamose, Ayoub Zeroual, Alexandre Roy, and Christophe Kinnard. "Impacts of Agricultural Areas on Spatio-Temporal Variability of Daily Minimum Extreme Flows during the Transitional Seasons (Spring and Fall) in Southern Quebec." Water 13, no. 24 (December 7, 2021): 3487. http://dx.doi.org/10.3390/w13243487.

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Several statistical methods were used to analyze the spatio-temporal variability of daily minimum extreme flows (DMEF) in 17 watersheds—divided into three homogenous hydroclimatic regions of southern Quebec—during the transitional seasons (spring and fall), during the 1930–2019 period. Regarding spatial variability, there was a clear difference between the south and north shores of the St. Lawrence River, south of 47° N. DMEF were lower in the more agricultural watersheds on the south shore during transitional seasons compared to those on the north shore. A correlation analysis showed that this difference in flows was mainly due to more agricultural areas ((larger area (>20%) on the south than on the north shore (<5%)). An analysis of the long-term trend of these flows showed that the DMEF of south-shore rivers have increased significantly since the 1960s, during the fall (October to December), due to an increase in rainfall and a reduction in cultivated land, which increased the infiltration in the region. Although there was little difference between the two shores in the spring (April to June), we observed a decrease in minimum extreme flows in half (50%) of the south-shore rivers located north of 47° N.
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5

Pouliot, Daniel, and Jean-François Desroches. "Découverte de la Salamandre à quatre orteils, Hemidactylium scutatum, à Québec, Québec : limite nord-est de l'espèce sur la rive nord du fleuve Saint-Laurent." Canadian Field-Naturalist 119, no. 1 (January 1, 2005): 129. http://dx.doi.org/10.22621/cfn.v119i1.91.

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Анотація:
En 1999 trois spécimens de Salamandre à quatre orteils ont été observés à Québec, sur la rive nord du fleuve Saint-Laurent. Des recherches effectuées au même site en 2001 ont permis de découvrir d’autres spécimens de même que des pontes. Ces mentions élargissent la distribution connue de l’espèce de 90 km vers le nord-est-est et 80 km vers le nord-nord-ouest. Il s’agit vraisemblablement de la limite nord-est de cette salamandre, sur la rive nord du Saint-Laurent.In 1999, three Four-toed Salamanders were observed at Québec, north shore of the St. Lawrence River. Field searches in 2001 allowed the discovery of another specimen as well as egg clutches. These records extend the known range of the species 90 km north-east-east and 80 km north-north-west. This is probably the northeastern limit of this salamander’s range on the north shore of St. Lawrence River.
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6

Roy, Gilles. "Une épidémie d’insectes, facteur de déboisement dans le Québec." Cahiers de géographie du Québec 2, no. 4 (April 12, 2005): 233–40. http://dx.doi.org/10.7202/020090ar.

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Spruce budworm bas invaded the forest of Québec since 1939, especially the pines of the coniferous area. There are jour major infested regions : three are located on the North shore of the St. Lawrence river : in the Gatineau river bassin, in the Laurentians between the Lachute Area and lake St. John, and in the North Shore region behind Baie Comeau Sept-Iles. The fourth region starts behind Rimouski and spreads eastward, covering the whole Gaspé peninsula. In this last the authorities are quite concerned about this plague, which is becoming a serious menace to the forest industries. Various air-spays have been used during the past jour years in order to circumscribe the dammages, and more than 4,000,000 acres have been treated with DDT, first step toward the rehabilitation of the forest.
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7

Rahmat, S. J., I. A. Koretsky, J. E. Osborne, and A. A. Alford. "New Miocene Monachinae from the Western Shore of the Chesapeake Bay (Maryland, USA)." Vestnik Zoologii 51, no. 3 (June 27, 2017): 221–42. http://dx.doi.org/10.1515/vzoo-2017-0029.

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Abstract The Family Phocidae includes four subfamilies (Phocinae, Monachinae, Cystophorinae, and Devinophocinae) consisting of mediumto large-sized mammals that possess distinctive adaptations to semi-aquatic life. In the Miocene of the Chesapeake Group, only two subfamilies of the Family Phocidae were identified: Phocinae and Monachinae. Leptophoca, a representative of the subfamily Phocinae, appears on the eastern shore of the North Atlantic around 16 million years ago. Recently, two new monachine species, the larger Terranectes magnus (n. gen., n. sp.) and the medium-sized T. parvus (n. sp.), were recorded in the Upper Miocene of the Chesapeake Group in the Eastover Formation (7.0–6.0 Ma) and St. Marys Formation (10.0-8.0 Ma). These two distinct subfamilies of seals indicate a well-marked divergence between phocines and monachines, much earlier than 18 million years ago, as previously suggested. The Eastover Formation was deposited in a shallow embayment that covered southern Maryland, the coastal plain of Virginia, and the northeastern corner of North Carolina. The geologically older St. Marys Formation represents a tide-influenced coastal environment, with low-salinity estuaries. There was a sharp temperature decrease in the Late Miocene, indicated by a shift to a cooler-water fish fauna during St. Marys time. The Eastover Formation reflects warmer waters with relatively strong currents, significant shoals, barriers, and varied depths. Fossil evidence of earlier seals suggests that phocids originated in the North Atlantic and otarioids in the North Pacific. True seals diverged from ancient Carnivora in the early Oligocene (or earlier) in the Paratethyan / Mediterranean Basins, spread widely during the Middle Miocene and crossed westward across the Atlantic Ocean, before dispersing in the eastern United States by the Early Pliocene.
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8

Pratte, Steve, Michelle Garneau, and François De Vleeschouwer. "Late-Holocene atmospheric dust deposition in eastern Canada (St. Lawrence North Shore)." Holocene 27, no. 1 (July 28, 2016): 12–25. http://dx.doi.org/10.1177/0959683616646185.

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Dust deposition in two ombrotrophic peatlands (Baie and Ile du Havre peatland (IDH) bogs) of the Estuary and Gulf of the St. Lawrence in eastern Canada was reconstructed using elemental geochemistry. The rare earth elements (REEs) and other lithogenic element concentrations were measured by ICP-oES and Q-ICP-MS along two peat cores spanning the last 4000 years. Principal component analyses on the geochemical profiles show that REEs display the same behavior as Al, Ti, Sc, and Zr, all conservative elements, which suggests that REEs are immobile in the studied peat bogs and can be used as tracers of dust deposition. Plant macrofossils were also used to infer past environmental and humidity changes. The dust fluxes were reconstructed using the sum of REEs (ΣREE). The range of dust deposition varies from 0.2 to 3.8 g m−2 yr−1 in the Baie bog, while the IDH bog shows lower fluxes ranging between 0.1 and 1.2 g m−2 yr−1. The highest dust fluxes in the Baie bog were recorded from 1750–1000 cal. BP to 600–100 cal. BP and occur at the same time as periods of high variability in the macrofossil record (i.e. successive layers dominated by Sphagnum or Ericaceae). The timing of these events in the dust and macrofossil records also corresponds to documented cold periods. These two periods have been identified as episodes of climatic instability, which could have been caused by changes in the wind regime.
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9

Dionne, Jean-Claude. "Les erratiques de dolomie à Rivière-Blanche, côte sud de l'estuaire maritime du Saint-Laurent : un indicateur de transport glaciaire et glaciel." Canadian Journal of Earth Sciences 39, no. 8 (August 1, 2002): 1239–55. http://dx.doi.org/10.1139/e02-009.

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At Rivière-Blanche, a locality on the south shore of the lower St. Lawrence estuary, the clayey and rocky shore zone is largely covered by stones of various sizes and lithologies, from local and far-distant sources. A survey exceeding 31 000 boulders indicates that 31% are Precambrian clasts (granite, gneiss, anorthosite, etc.) from the Canadian Shield located on the north shore of the St. Lawrence, 40 km from Rivière-Blanche, and 69% are Appalachian lithologies, mainly (45%) sandstone and graywacke. There are also 1.5% of dolostone erratics, a lithology not widespread in the Canadian Shield nor in the Appalachians. Of the 1242 clasts of the various varieties of dolostone erratics observed, the grey coral (Cladopora) dolostone erratics are restricted to the Rivière-Blanche area, whereas many other varieties are common to both shores of the St. Lawrence estuary. The most likely far-distance source is the Proterozoic Mistassini sedimentary basin, while a few varieties such as the coral dolostone erratics are from the Appalachian Siluro-Devonian formations, of which the nearest outcrops are located in the northwestern area of Lake Matapedia, 25–30 km south of Rivière-Blanche. Whatever their source, the dolostone erratics were first transported by a late Wisconsinian regional ice stream before being released by icebergs in the Goldthwait Sea. The coral dolostone (Clapodora) erratics provide additional evidence for a northward ice flow between Lake Matapedia and Rivière-Blanche during an early phase of deglaciation of the St. Lawrence Valley after the formation of an Appalachian ice divide located approximately at the latitude of Lac-au-Saumon.
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10

Magnan, Gabriel, Michelle Garneau, and Serge Payette. "Holocene development of maritime ombrotrophic peatlands of the St. Lawrence North Shore in eastern Canada." Quaternary Research 82, no. 1 (July 2014): 96–106. http://dx.doi.org/10.1016/j.yqres.2014.04.016.

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AbstractMacrofossil analyses were used to reconstruct long-term vegetation successions within ombrotrophic peatlands (bogs) from the northern shorelines of the St. Lawrence Estuary (Baie-Comeau) and the Gulf of St. Lawrence (Havre-St-Pierre). Over the Holocene, the timing and the ecological context of peatland inception were similar in both regions and were mainly influenced by fluctuations in relative sea level. Peat accumulation started over deltaic sands after the withdrawal of the Goldthwait Sea from 7500 cal yr BP and above silt–clay deposits left by the Laurentian marine transgression after 4200 cal yr BP. In each region, the early vegetation communities were similar within these two edaphic contexts where poor fens with Cyperaceae and eastern larch (Larix laricina) established after land emergence. The rapid transitions to ombrotrophy in the peatlands of Baie-Comeau are associated with particularly high rates of peat accumulation during the early developmental stage. The results suggest that climate was more propitious to Sphagnum growth after land emergence in the Baie-Comeau area. Macrofossil data show that treeless Sphagnum-dominated bogs have persisted over millennia and that fires had few impacts on the vegetation dynamics. This study provides insight into peatland vegetation responses to climate in a poorly documented region of northeastern America.
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Дисертації з теми "North Shore of the St"

1

Boyne, Andrew W. "Diet and reproductive success of Herring Gulls nesting on the middle north shore of the Gulf of St. Lawrence." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk2/ftp03/MQ50725.pdf.

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2

Boyne, Andrew. "Diet and reproductive success of herring gulls nesting on the middle north shore of the Gulf of St. Lawrence." Thesis, McGill University, 1999. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=21516.

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Анотація:
Breeding biology and diet of Herring Gulls Larus argentatus were studied on Ile Nue, in the Mingan Archipelago National Park Reserve, in the Gulf of St. Lawrence. Nesting parameters were measured 1994--1996, and fledging success and diet were followed in 1996. Clutch size was low in all three years of the study, and hatching success was low in 1995. Low clutch size and hatching success could not be explained by researcher disturbance, predation, or competition for nest sites, leaving food-stress as the most likely explanation. To reduce the biases associated with determining diet, we used four methods to estimate diet. The 1996 breeding season was divided into three periods using changes in the number of gulf pellets collected from roost sites as an indirect measure of dietary changes; these periods corresponded to the pre-spawning, spawning, and post-spawning periods of capelin Mallotus villosus. (Abstract shortened by UMI.)
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3

Dietrich, Pierre. "Faciès, architectures stratigraphiques et dynamiques sédimentaires en contexte de régression forcée glacio-isostatique : la réponse pro- à paraglaciaire des complexes deltaïques de la Côte Nord de l'Estuaire et du Golf du Saint-Laurent (Québec, Canada)." Thesis, Strasbourg, 2015. http://www.theses.fr/2015STRAH019/document.

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Анотація:
La Côte Nord de l’Estuaire et du Golfe du St. Laurent (Québec, Canada) est caractérisée par une série de complexes deltaïques mis en place en contexte de chute de Niveau Marin Relatif (NMR) forcée par le rebond glacio-isostatique, lors du retrait des marges de l’Inlandsis Laurentidien. L’étude de trois complexes deltaïques montre qu’un motif d’évolution morphostratigraphique contrôlé par le retrait des marges glaciaires prévalait au premier ordre. Le premier stade de sédimentation se caractérise par la mise en place de cônes d’épandage juxtaglaciaires sous-aquatiques. Leur localisation au front de la marge glaciaire fait que la répartition spatiale des corps sédimentaires montre localement un empilement en rétrogradation. Dès l’émergence d’un front glaciaire continental, des deltas proglaciaires se développent en contexte de chute de NMR, formant des lobes dont l’altitude décroît vers le bassin. Ces derniers sont initialement associés à un système fluviatile en tresse alimenté en sédiments glaciogéniques par les marges glaciaires en retrait. Malgré des taux de chute de NMR de plusieurs cm/an, aucune incision fluviatile n’est observée à ce stade et la dynamique de transfert est prédominante du fait des forts taux d’apports sédimentaires. Plus tard, à la suite du retrait des marges glaciaires hors des bassins versants, le remaniement paraglaciaire se développe du fait de la réduction drastique des apports en eaux et sédiments. Le système fluviatile, devenu méandriforme, s’encaisse dans les anciens dépôts deltaïques maintenant inactifs et les bordures de deltas sont remaniées par les processus littoraux (plages soulevées, terrasses marines). Cette étude révèle que la majorité du volume de ces complexes deltaïques (10-20 km3) est mis en place en quelques milliers d’années seulement, immédiatement après la déglaciation ; le remaniement paraglaciaire n’ayant contribué à l’accrétion deltaïque que très marginalement. La modélisation numérique (Dionisos) valide les différents forçages identifiés par l’analyse morphosédimentaire. Une synthèse des complexes deltaïques à l’échelle de toute la Côte Nord du St. Laurent a permis de catégoriser 21 complexes deltaïques en 4 scénarios d’évolution morphosédimentaire, directement liés à la dynamique de retrait de la marge glaciaire. Leur décryptage offre une clef de lecture originale pour l’historique du retrait des marges glaciaires de l’Inlandsis Laurentidien sur la période 12-7.5 ka cal BP
The North Shore of the St. Lawrence Estuary and Gulf is characterized by the presence of deltaic complexes that were emplaced under falling Relative Sea Level (RSL) forced by the glacio-isostatic rebound, immediately after the retreat of the Laurentide Ice Sheet (LIS) margin. The study of three deltaic complexes reveals that a common morphostratigraphic evolution forced by the retreat of the LIS prevailed for the edification of these structures, reflecting the retreat of the LIS margin. The emplacement of subaqueous outwash fans beyond the retreating or stillstanding glaciomarine margin constitutes the first stage of this evolution. As tied to the ice-margin position, these fans are characterized in places by a backstepping stacking pattern, in spite of the forced regressive setting. From the emergence of a continental ice front, the proglacial deltaic system develops and forms lobes staged accordingly to the RSL fall. These deltaic systems actively prograde at that time because they are fed in glaciogenics by the retreating LIS margin through braided meltwater streams. In spite of the RSL fall reaching several centimeters per years, no fluvial entrenchment occurs mainly owing to the significant amount of sediment supply. Later, when the LIS margin retreats from the drainage basins of feeding rivers, fluvial systems experience a drastic drop in sediment supply that forced the interruption of the deltaic progradation and the onset of paraglacial reworking. The paraglacial reworking consists in the entrenchment of a meandering fluvial system within former deltaic deposits and shows the prevalence of shallow-marine processes (waves, tides) at the delta rim (raised beaches, marine terraces). This study reveals that the bulk of the deltaic volume (c.a. 10-20 km3) for each complex was emplaced in only a few thousands of years following the LIS margin retreat when the latter was still located in the drainage basin. The paraglacial reworking had a minor influence on the deltaic accretion. A forward stratigraphic model (Dionisos) is used to validate the variety of forcing as understood from the sedimentary analysis. A synthesis including 21 deltaic complexes of the St. Lawrence North Shore allowed the establishment of a fourfold categorization. This scheme of deltaic evolution was used in order to refine the position of the LIS margin retreating upland for a period ranging from 12 to 7.5 ka cal BP
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4

Brionne, Charles. "Signatures morphosédimentaires de la dynamique juxta-glaciaire à la transition de fronts glaciaires marins à terrestres : le cas de la Côte-Nord du Québec (estuaire et golfe du St Laurent)." Electronic Thesis or Diss., Strasbourg, 2024. http://www.theses.fr/2024STRAH005.

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Анотація:
Cette thèse combine une double approche géomorphologique et sédimentologique associée à l’utilisation de données LiDAR, bathymétriques, photogrammétrie drone et de datations radiocarbones. Elle a permis de reconstituer les paléos dynamiques glaciaires en contexte de déglaciation pour l’Inlandsis Laurentidien depuis le dernier maximum glaciaire, il y a environ 20 000 ans, et plus précisément au passage d’une marge glaciaire ancrée en mer à une marge glaciaire continentale Deux études ont été menées conjointement, soit : (1) la cartographie, la synthèse et la proposition d’un modèle concernant les mégacannelures de la Côte-Nord du Saint-Laurent, une première pour ces morphologies et (2) la reconstruction de l’enregistrement géomorphologique et morphosédimentaire du complexe sédimentaire de Pentecôte, mimant précisément cette transition. D’une manière générale, cette thèse démontre l’importance de l’héritage structural et de la physiographie du plancher au marge glaciaire dans la reconstruction de la dynamique glaciaire de retrait de la marge du LIS oriental
This thesis combines a dual geomorphological and sedimentological approach with the use of LiDAR data, bathymetry, drone photogrammetry and radiocarbon dating. It has enabled us to reconstruct the glacial paleodynamics in a deglaciation context for the Laurentide ice sheet since the last glacial maximum, around 20,000 years ago, and more specifically during the transition from an ice margin anchored at sea to a continental ice margin: (1) mapping, synthesising and proposing a model for the megagrooves of the North Shore of the St Lawrence, a first study for these morphologies, and (2) reconstructing the geomorphological and morphosedimentary record of the Pentecôte sedimentary complex, which precisely represents this transition. Overall, this thesis demonstrates the importance of the structural heritage and physiography of the floor at the glacial margin in the reconstruction of the glacial retreat dynamics of the eastern LIS margin
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5

Spake, Phillip. "Geothermal Exploration North of Mount St. Helens." Master's thesis, Temple University Libraries, 2019. http://cdm16002.contentdm.oclc.org/cdm/ref/collection/p245801coll10/id/585881.

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Анотація:
Geology
M.S.
Active seismicity and volcanism north of Washington state’s Mount St. Helens provide key ingredients for hydrothermal circulation at depth. This broad zone of seismicity defines the St. Helens Seismic Zone, which extends well north of the volcanic edifice below where several faults and associated fractures in outcrop record repeated slip, dilation, and alteration indicative of localized fluid flow. Candidate reservoir rocks for a geothermal system include marine metasediments overlain by extrusive volcanics. The colocation of elements comprising a geothermal system at this location is tested here by analysis of the structures potentially hosting a reservoir, their relationship to the modern stress state, and temperature logs to a depth of 250 m. Outcrop mapping and borehole image log analysis down to 244 m document highly fractured volcaniclastic deposits and basalt flows. Intervening ash layers truncate the vertical extent of most structures. However, large strike slip faults with well-developed fault cores and associated high fracture density cross ash layers; vein filling and alternation of the adjacent host rock in these faults suggest they act as vertically extensive flow paths. These faults and associated fractures record repeated slip, dilation, and healing by various dolomite, quartz, and hematite, as well as clay alteration, indicative of long-lived, localized fluid flow. In addition, where these rocks are altered by igneous intrusion, they host high fracture density that facilitated heat transfer evidenced by associated hydrothermal alteration. Breakouts in image logs indicate the azimuth of SHmax in the shear zone is broadly consistent with both the GPS plate convergence velocity field as well as seismically active strike slip faults and strike-slip faults mapped in outcrop and borehole image logs. However, the local orientation of SHmax varies by position relative to the edifice and in some cases with depth along the borehole making a simple regional average SHmax azimuth misleading. Boreholes within the seismic zone display a wider variety of fracture attitudes than those outside the shear zone, potentially promoting permeability. Temperature profiles in these wells all indicate isothermal conditions at average groundwater temperatures, consistent with rapidly flowing water localized within fractures. Together, these results indicate that the area north of Mount Saint Helens generates and maintains porosity and permeability suggesting that conditions necessary for a geothermal system are present, although as yet no modern heat source or hydrothermal circulation was detected at shallow depth.
Temple University--Theses
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6

Billot, Jennie Margaret. "Women's agency in the North Shore and Waitakere cities of Auckland (New Zealand)." Thesis, University of Auckland, 1998. http://wwwlib.umi.com/dissertations/fullcit/9908064.

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This thesis examines the ways in which women assess and seek resources in their urban contexts. I argue that the struggles of daily life in local communities and institutional groups can produce ideological spaces into which new practices, arising from increased consciousness of issues, can be developed. My aim has been to uncover women's experiences in a way that not only interprets meanings from their practices, but also encourages such practices to be seen as valid renderings of women's understandings. I examine women's initiatives through the analysis of varying contexts. While I acknowledge the historical importance of the domestic situation as a threshold for much historic activism, women's proactivity requires a broader situational analysis. I therefore present cases of proactivity within the domestic, public and business spheres, within the two cities of Waitakere and North Shore of Auckland, New Zealand. Through the search for new progressive social identities, women's activities at the inter-personal level are a prime source of social change. It is through the recursive relationship between women as agents and the social structure, that changing interpretations of social expectations are produced, allowing for creative activism. While women's initiatives may aim to transform particular social environments, they become part of the incremental process of change that alters the experience and structure of women's lives. The thesis has four parts. The first outlines the scope, objectives and theoretical framework, while the second conceptualises women's agency and its positioning within social gendered structures. Part Three presents the investigative processes linking the theoretical framework and the empirical analysis. Part Four submits the thematic interpretations of the thesis, concluding that women can be agents of social change in a diversity of ways. I acknowledge my feminist stance, one with layerings of objectives and motivations. I view women's circumstances as resulting from the interweaving of structural forces and personal capacities. The resulting awareness of women's experiences can challenge the values and concepts of masculine discourses. This is viewed through the concept of multiplicity. On a political level this means creating a resistance to hierarchies and a commitment to a plurality of voice, style and structure.
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7

Markus, Felicia. "Living on another shore : early Scandinavian settlement on the North-Western Estonian coast /." Uppsala : Department of Archaeology and Ancient History, Uppsala University [Institutionen för arkeologi och antik historia, Uppsala universitet], 2004. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-4717.

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8

Lapierre, Christine. "Shop-floor society : work and social relations on the North Shore of Québec." Thesis, McGill University, 2005. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=83191.

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Iron Bay is a small community situated on the North Shore of the province of Quebec, where people work mainly in the resources and industrial sectors. This study examines the social relations of the workers of an iron pellet plant in that community, both at work and outside. The social organization of work, the relations between hierarchical orders at work and leisure activities are examined to produce an ethnographic account of the way of life of an affluent, if isolated, segment of the working class of Quebec.
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9

Calliari, Lauro Julio. "Cross-shore and longshore sediment size distribution on southern Currituck Spit, North Carolina." W&M ScholarWorks, 1990. https://scholarworks.wm.edu/etd/1539616594.

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Using Q-mode factor analysis, 87 surficial sediment samples collected from Duck and Whalehead beach, North Carolina, were analyzed using the weight percent of the gravel and sand fraction subdivided at 0.5 phi class interval as variables. An additional data set composed of 178 surficial sediment samples from Duck beach (bimodal) and Coquina beach (unimodal fine) representing three years of sampling at monthly intervals were analyzed by the same technique using only the sand fraction. The spatial and temporal patterns of sediment factor groups support three main inferences. (1) Bimodal beaches display a more distinct sediment zonation than unimodal beaches. (2) On a long term basis (yearly), cross-shore grain-size distributions represent depositional processes. Particularly on bimodal beaches, the association of sediment factor groups with specific zones of the beach profile delineates a textural differentiation produced by the type and amount of energy inherent in each zone. Combinations of Q-mode factor analysis and other environmental sensitive techniques (e.g. log-probability plots of grain-size distributions) proved to be useful for interpreting sedimentary processes at the depositional site. (3) The cross-shore patterns which represent an average of the sedimentary processes occurring under fair weather and storm conditions indicate that coarse sediments are concentrated on the backshore. In contrast, fine sediments are located landward or shoreward of this zone where they are exposed to energy conditions that result in their depletion in the subaerial beach. Using the Q-mode factor model, 350 new sediment samples from beaches located between Duck and Oregon Inlet were "mapped" in the factor space defined by the Duck-Coquina data set. The along-coast results support the cross-shore trends observed in the previous studies and indicates that there are several sources of coarse sediments between Duck and Oregon Inlet. Sedimentologic, stratigraphic and seismic data offshore and landward of the barrier substantiate these findings and demonstrate that differences in subaerial beach morphology in this part of Currituck Spit, is primarily due to the availability of coarse sediments from the paleodrainage of the Albemarle river.
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10

Longo, Matthew. "Reciprocal with the landscape : observations and transformation of village form in the North Shore." Thesis, Massachusetts Institute of Technology, 1985. http://hdl.handle.net/1721.1/31001.

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Thesis (M.Arch.)--Massachusetts Institute of Technology, Dept. of Architecture, 1985.
MICROFICHE COPY AVAILABLE IN ARCHIVES AND ROTCH.
Bibliography: p. 155-160.
The purpose of this thesis is to suggest an alternative way of responding to context in architectural design. The thesis is an exploration in how the formal structure of a place influences the experience of that place, and how these principles of formal structure can, in turn, be incorporated into contemporary architecture. The goal of the thesis is to move beyond the image of a place and emphasize the essential quality of human "scale / size". This quality is in the form of the villages of the North Shore. The work here is an attempt to show that by identifying these underlying principles that build the form of these villages, contemporary architecture can be designed to reinforce the same positive associations found in the village form. The thesis has three parts: I. Observation Studies -- Four village streets are documented and formal structure analyzed. II. Principles for Building t he Hater's Edge -- A discussion about transformation of observations and formal principles into contemporary form. III. Design Studies -- Manchester Waterfront is the site selected to explore the principles of formal structure using a mixed use program for a commercial development.
by Matthew Longo.
M.Arch
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Книги з теми "North Shore of the St"

1

Wild, Kenneth S. Archeological investigations conducted along the North Shore Road, St. John, U.S. Virgin Islands. Tallahassee, Fla: National Park Service, Southeast Archeological Center, 1986.

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2

Assembly, Canada Legislature Legislative. Bill: An act to incorporate the "St. La[wrence] North Shore Navigation Company". Quebec: Thompson, 2003.

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3

Petricevich, Colleen. St. Joseph's Takapuna, 1966-2006: 40 year history : St Joseph's Catholic Church, 1966-2006. Edited by St. Joseph's Parish (North Shore City, N.Z.). North Shore City, N.Z: St Joseph's Parish, 2007.

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4

Fitzhugh, William W. Archaeological survey of the Quebec lower north shore, Gulf of St. Lawrence, from Mingan to Blanc Sablon. Washington, D.C.]: Arctic Studies Center, 2002.

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Assembly, Canada Legislature Legislative. Bill: An act to extend the period fixed for the completion of their works by the North Shore Railway and St. Maurice Navigation and Land Company. Quebec: Thompson, Hunter, 2003.

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6

Assembly, Canada Legislature Legislative, ed. Petition of the Montagnais tribe of Indians, inhabiting the north shore of the St. Lawrence, or territory formerly designated by the name of the "King's Posts". [S.l: s.n., 1985.

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7

Porter, Russ. North Shore/South Shore. Forest Park, Ill: Heimburger House Pub. Co., 1999.

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8

McQuarrie, Willis John. True tall tales of Algoma-Manitoulin: 400 fascinating stories of happenings from communities along the North Shore, St. Jos. Island, the Manitoulin and Cockburn Islands, and areas. [Gore Bay, Ont: W.J. McQuarrie, 2006.

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9

McQuarrie, Willis John. True tall tales of Algoma-Manitoulin: 400 fascinating stories of happenings from communities along the North Shore, St. Jos. Island, the Manitoulin and Cockburn Islands, and areas. [Gore Bay, ON: W.J. McQuarrie, 2007.

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10

Penna, Robin. A short guide to Port Isaac, Port Gaverneand Trelights in the parish of St. Endellion, North Cornwall. 2nd ed. Port Isaac: Blackthorn Press, 1991.

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Частини книг з теми "North Shore of the St"

1

Davis, Loren G. "The North American Paleocoastal Concept Reconsidered." In Trekking the Shore, 3–26. New York, NY: Springer New York, 2011. http://dx.doi.org/10.1007/978-1-4419-8219-3_1.

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2

Haras, W. S. "Canada--Lake Erie: North Shore." In The GeoJournal Library, 467–74. Dordrecht: Springer Netherlands, 1988. http://dx.doi.org/10.1007/978-94-009-2999-9_50.

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3

Dietrich, Pierre, Alexandre Normandeau, Patrick Lajeunesse, Jean-François Ghienne, Mathieu Schuster, and Alexis Nutz. "Deltaic Complexes of the Québec North Shore." In World Geomorphological Landscapes, 245–58. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-35137-3_10.

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4

Steele, Teresa E., and Esteban Álvarez-Fernández. "Initial Investigations into the Exploitation of Coastal Resources in North Africa During the Late Pleistocene at Grotte Des Contrebandiers, Morocco." In Trekking the Shore, 383–403. New York, NY: Springer New York, 2011. http://dx.doi.org/10.1007/978-1-4419-8219-3_16.

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5

Walkden, Mike, Mark Dickson, James Thomas, and Jim W. Hall. "Simulating the Shore and Cliffs of North Norfolk." In Advances in Global Change Research, 187–211. Dordrecht: Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-007-5258-0_7.

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6

Joeris, Leonard S. "Lake Kariba: the Undp Program and North Shore." In Man-Made Lakes: Their Problems and Environmental Effects, 143–47. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm017p0143.

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7

Di Salvo, Maria. "A Venice of the North? Italian Views of St Petersburg." In St Petersburg, 1703–1825, 71–79. London: Palgrave Macmillan UK, 2003. http://dx.doi.org/10.1057/9781403937469_5.

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8

Arnold, Ellen. "Saints on the Shore: Coastal Encounters in the Early Medieval West." In Environmental Histories of the North Atlantic World, 15–24. Turnhout, Belgium: Brepols Publishers, 2023. http://dx.doi.org/10.1484/m.ehnaw-eb.5.131269.

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9

O’Connor, British. "Diabetes and Cardiovascular Disease Brian O’Connor North Shore Health Region Vancouver." In Diabetes and Cardiovascular Disease, 367–71. Boston, MA: Springer US, 2001. http://dx.doi.org/10.1007/978-1-4615-1321-6_46.

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10

Witthuhn, Kathleen. "The Response to Rifting by the North Shore Volcanics in Minnesota." In Basement Tectonics 10, 41–45. Dordrecht: Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-017-0831-9_9.

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Тези доповідей конференцій з теми "North Shore of the St"

1

Evans, Kevin Ray, and Robert T. Pavlowsky. "RAISED SHORE PLATFORMS AND AN EARLY JAMAICAN POTSHERD IN SOUTHWESTERN ST. ELIZABETH PARISH: NEOTECTONIC IMPLICATIONS FOR AN ARCHAEOLOGICAL HYPOTHESIS." In 54th Annual GSA North-Central Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020nc-348135.

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2

Butter, M. "Development of Field Rehabilitation Plan for Mature Oilfield on Shore Azerbaijan." In 2nd EAGE St Petersburg International Conference and Exhibition on Geosciences. European Association of Geoscientists & Engineers, 2006. http://dx.doi.org/10.3997/2214-4609-pdb.20.p028.

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3

Osman, H., and M. Neyazy. "Off-Shore Mediterranean Sea Oil Potential, Egypt." In 1st EAGE North African/Mediterranean Petroleum & Geosciences Conference & Exhibition. European Association of Geoscientists & Engineers, 2003. http://dx.doi.org/10.3997/2214-4609-pdb.8.t032.

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4

Bonin, B. J., Greg Brick, and Carrie Jennings. "BEDROCK COLLAPSE IN ST. PETER SANDSTONE." In 54th Annual GSA North-Central Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020nc-347806.

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5

Evans, Kevin Ray, Toby Dogwiler, Douglas J. Faulkner, Peter M. Jacobs, Brett Kenning, Scott A. Lecce, and Robert T. Pavlowsky. "LATE HOLOCENE RAISED SHORE PLATFORMS IN SOUTHWESTERN JAMAICA." In 52nd Annual North-Central GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018nc-312468.

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6

Mwakanyamale, Kisa E., Steven E. Brown, and Ethan J. Theuerkauf. "MODELING EROSION AND ACCRETION ALONG THE ILLINOIS LAKE MICHIGAN SHORE." In 52nd Annual North-Central GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018nc-313264.

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7

Nicotra, Giacomo, Francesco Dresda, Antonio Tignanelli, William James Moore, and Vincewzo Michetti. "Key Drivers Determination for Off-shore Facilities Decommissioning and Abandonment Cost Estimate." In North Africa Technical Conference and Exhibition. Society of Petroleum Engineers, 2010. http://dx.doi.org/10.2118/127412-ms.

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8

Walkden, Mike, Mark Dickson, James Thomas, and Jim Hall. "PROBABILISTIC SIMULATION OF LONG TERM SHORE MORPHOLOGY OF NORTH NORFOLK UK." In Proceedings of the 31st International Conference. World Scientific Publishing Company, 2009. http://dx.doi.org/10.1142/9789814277426_0362.

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9

Поморцев, О., O. Pomorcev, А. Поморцева, and A. Pomorceva. "About the Global Fluvial Cycle of North Asia Sedimentogenesis." In XXVII International Shore Conference "Arctic Coast: The Path to Sustainability". Academus Publishing, 2019. http://dx.doi.org/10.31519/conferencearticle_5cebbb8cee4602.44595304.

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10

Miller, James D., and John C. Green. "TEACHING THE GEOLOGIC HERITAGE OF MINNESOTA’S NORTH SHORE AT THE NORTH HOUSE FOLK SCHOOL, GRAND MARAIS." In 54th Annual GSA North-Central Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020nc-348058.

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Звіти організацій з теми "North Shore of the St"

1

Rogers, Caroline. A synthesis of coral reef research at Buck Island Reef National Monument and Salt River Bay National Historical Park and Ecological Preserve, St. Croix, U.S. Virgin Islands: 1961 to 2022. National Park Service, September 2022. http://dx.doi.org/10.36967/2294235.

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This synthesis focuses on the history of research on coral reefs within two U.S. National Park Service units in St. Croix, U.S. Virgin Islands: Buck Island Reef National Monument (from 1961 to 2022) and Salt River Bay National Historical Park and Ecological Preserve (from 1980 to 2022). Buck Island Reef National Monument (BUIS) is off the north shore of the island of St. Croix, in the U.S. Virgin Islands. Established in 1961 and expanded in 2001, it is under the jurisdiction of the National Park Service (NPS). Long-term monitoring programs maintained by the NPS and jointly by the University of the Virgin Islands (UVI) and the Virgin Islands Department of Planning and Natural Resources (VIDPNR) provide data on trends in living coral cover and specific coral species from 2000 and 2001, respectively. Disease, thermal stress (indicated by coral bleaching), and hurricanes reduced total coral cover periodically, but cover remained relatively stable from 2007 through the end of 2020. Salt River Bay National Historical Park and Ecological Preserve (SARI) is a national park on the north shore of the island of St. Croix, in the U.S. Virgin Islands. Established in 1992, it is co-managed by the NPS and the Government of the Virgin Islands. Long-term monitoring programs maintained by the NPS and by the UVI with the VIDPNR provide data on trends in living coral cover and individual coral species from 2011 and 2001, respectively. In spite of thermal stress (indicated by coral bleaching), disease, and hurricanes, total coral cover remained relatively stable through the end of 2020. This document also includes results from extensive investigations by the National Oceanic and Atmospheric Administration (NOAA) and from many individual projects including those based out of the underwater saturation habitats Hydrolab and Aquarius from 1977 to 1989, as well as studies from researchers at Fairleigh Dickinson University’s West Indies Laboratory. While not possible to review all of these in detail, this report highlights information considered useful to managers, and scientists planning future research. In 2021, a particularly virulent disease called stony coral tissue loss disease (SCTLD), first noted in 2014 in Florida, and then in 2019 in the U.S. Virgin Islands, started killing corals in BUIS and SARI with the different species showing a gradient of susceptibility. An exact cause or link between this disease and human actions has not been discovered to date. The losses associated with this disease have now exceeded those from any other stressors in these national parks.
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2

Farahbod, A., and J. F. Cassidy. Spatial and temporal variations in seismic coda Q attenuation in the lower St. Lawrence region, southeastern Quebec. Natural Resources Canada/CMSS/Information Management, 2023. http://dx.doi.org/10.4095/332027.

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We investigate seismic attenuation characteristics of the Lower St. Lawrence seismic zone in southeastern Quebec. This zone is located ~400 km downstream from Quebec City and is between the Quebec North Shore and the Lower St. Lawrence. We used earthquake recordings from 5 broadband and 5 short period seismograph stations of the Canadian National Seismic Network (CNSN) across the region. Our dataset is comprised of 847 earthquakes recorded between 1985 and 2022 with magnitudes ranging from 2.0 to 5.1, depths from 0 to 30 km and epicentral distances of 5 to 100 km. This gives a total of 446 high signal-to-noise (S/N) traces (S/N?5.0) useful for QC calculation (with a maximum ellipse parameter, a2, of 100) across the region. Coda windows were selected to start at tc = 2tS (two times the travel time of the direct S wave), and were filtered at center frequencies of 2, 4, 8, 12 and 16 Hz. Our study reveals a consistent pattern. We find that the lowest overall average of Q0 (Q at 1 Hz) values are at the three stations (GSQ, ICQ and SMQ) within 100 km of a moderate earthquake of mN 5.1 in 1999 (e.g., Q0 of 81, 88 and 80, respectively). We determined temporal variations in attenuation following the 1999 earthquake. The overall average of Q0 decreased from 87 (before the mainshock) to 77 (GSQ, D=96 km), from 92 to 85 (ICQ, D=69 km) and from 88 to 82 (SMQ, D=73 km). These results are in agreement with global studies that show a decrease in Q0 following a significant earthquake, (e.g., M &amp;gt; 5) likely the result of increased fracturing and fluids in the epicentral region. An average for all the data results in a Q relationship of QC = 86f1.07 for the frequency band of 2 to 16 Hz for the entire region.
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3

Wilson, Aixa, Aaron Deter-Wolf, Benjamin D. Maygarden, and Mary E. Weed. Cultural Resources Survey, Lake Pontchartrain West Shore Hurricane Protection Project, St. John and St. Charles Parishes, Louisiana. Fort Belvoir, VA: Defense Technical Information Center, August 2003. http://dx.doi.org/10.21236/ada417772.

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4

Davidson, A., and K. M. Bethune. Geology of the north shore of Georgian Bay, Grenville Province of Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1988. http://dx.doi.org/10.4095/122626.

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5

Kurfurst, P. J. Geotechnical Investigations of the Near - Shore Zone, North Head, Richards Island, N.W.T. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1986. http://dx.doi.org/10.4095/130150.

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6

Pearson, W. N., R. E. Bretzlaff, and J. J. Carrière. Copper deposits and occurrences in the north shore region of Lake Huron, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1985. http://dx.doi.org/10.4095/120312.

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7

Friske, P. W. B. Regional geochemical reconnaissance: interpretation of data from the north shore of Lake Superior. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1985. http://dx.doi.org/10.4095/120335.

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8

Morang, Andrew, Lauren Dunkin, David Bucaro, John Wethington, Michael Chrzastowski, and Ethan Theuerkauf. Sediment budget for the North Illinois Shore from the Wisconsin border to Wilmette Harbor. Engineer Research and Development Center (U.S.), August 2019. http://dx.doi.org/10.21079/11681/33679.

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9

Sinclair, Donna. Contested Visions of Place: People, Power, and Perception on the Columbia's North Shore, 1805-1913. Portland State University Library, January 2000. http://dx.doi.org/10.15760/etd.3066.

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10

Erickson, Zachary K., Erik Fields, Melissa M. Omand, Leah Johnson, Andrew F. Thompson, Eric D’Asaro, Filipa Carvalho, et al. EXPORTS North Atlantic eddy tracking. NASA STI Program and Woods Hole Oceanographic Institution, November 2022. http://dx.doi.org/10.1575/1912/29464.

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The EXPORTS North Atlantic field campaign (EXPORTS-NA) of May 2021 used a diverse array of ship-based and autonomous platforms to measure and quantify processes leading to carbon export in the open ocean. The success of this field program relied heavily on the ability to make measurements following a Lagrangian trajectory within a coherent, retentive eddy (Sections 1, 2). Identifying an eddy that would remain coherent and retentive over the course of a monthlong deployment was a significant challenge that the EXPORTS team faced. This report details the processes and procedures used by the primarily shore-based eddy tracking team to locate, track, and sample with autonomous assets such an eddy before and during EXPORTS-NA.
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